|
|
Base Model:
SRR-1 Model
click here for enlarged view [+]
| |
|
|
|
Scroll down to see a list of Available
Models and Key
Features for the Seismic Refraction / Seismic Reflection test
method.
Save money! Contact Olson Instruments when adding on to an existing
system, or purchasing multiple systems as some of the components
are common to other test methods.
|
|
|
|
|
Seismic Refraction investigations are commonly used to determine
bedrock depth & rippability.
Seismic Reflection surveys are
used to map, detect, & delineate geologic conditions including the
bedrock surface, voids, water table and layer geometry (folds).
The Seismic Refraction & Reflection (SRR) system is
designed to allow for either seismic refraction or seismic reflection
data acquisition. The SRR system, which is designed for shallow
surveys, can also be used for detecting voids in large civil structures
such as dams (seismic reflection).
Seismic Refraction surveys are used for excavation
purposes to map the bedrock depth and evaluation rock rippability.
Seismic refraction measurements are applicable in mapping subsurface
conditions for various uses including geologic, geotechnical,
hydrologic, environmental, mineral exploration, petroleum exploration,
and archaeological investigations. Seismic Refraction
investigations are commonly used to determine layer thickness and/or
the subsurface compressional wave velocity of the
overburden and underlying bedrock or to water table, stratigraphy,
lithology, structure, and fractures. This inherently shallow
technique requires that compressional seismic wave velocities increase
with depth so wave refraction occurs.
Seismic Reflection surveys are used to map, detect, and delineate
geologic conditions including the bedrock surface, confining layers
(aquitards), faults, lithologic stratigraphy, voids, water table,
fracture systems, and layer geometry (folds). This methodology requires
that the target be sufficiently deep, so that the incoming reflected
wave arrives after the surface wave generated from the impact. Near-surface
seismic-reflection data are generally high-resolution (dominant
frequency above 80 Hz) and image depths from around 20 ft (6 m)
to as much as several hundred feet (100+ meters).
Training
Hands-on training is available for all of our Nondestructive Testing
Methods at our Wheat Ridge, Colorado (USA) location, which is a
suburb located appromately 15 minutes northwest of downtown Denver. Training
may be available at your location by one of our agents upon special arrangement.
For complete details about the Seismic Reflection / Seismic Refraction system
available as an add-on test for the Freedom
Data PC platform, call toll free
1-888-423-1214 or email:
details@olsoninstruments.com
|
|
|
| |
Applicable On:
- Mass Concrete
- Mass Cyclopean Masonry
- Rock
- Soil
|
|
|
| |
Test For:
- Layer Thickness
- Bedrock Topography
- Water Table Depth/Mapping
- Compressional Wave Velocity Profiles
- Rippability/Excavatability
- Fractures, etc.
|
|
| |
Meets ASTM:
Meets ACI:
|
|
|
|
|
| |
All of Olson Instruments have been researched, tested, and used on-site daily
by our sister company, Olson
Engineering, world reknowned for NDT consulting. The OE
Website is loaded with Tech Brief and project photos using the
equipment shown on this website. Purchase our products to “do-it-yourself”,
or hire an Olson Engineering Nondestructive Testing professional for your
next project
|
|
|
|